Preface

In the
next two episodes of our Mineral-of-the-Month we will be visiting Petrified Wood.Not just
on the surface, but deep within this ancient woods cells.Part I will cover the chemistry and science
of what makes it, i.e., the process of petrification, its geology, and what
gives it its array of colors.
We will see some lapidary examples, as well.And,
we will begin nearest our clubhouse in the United
States to trek our petrified forests.

In part II, we will go into paleobotany, more lapidary uses, lore and metaphysical
applications, and
travel internationally, to see what the rest of the world proudly offers as paleo-beauty
from their homes,
as well.

So, put on your hardhat and safety sunglasses.Were
off to explore the many preserves of ancient
flora.Lets go!

Introduction

Good
morning!I hope you are all ready for our
excursion into sunny petwood country.As your
guide,
I will suggest places for us to collect, or in the case of special parks and preserves, to
just soak in the
multi-hued beauty of stony logs and trunks, to be admired where they fell a long time ago.

As there are several public and private locations for us to visit on our itinerary,
well have to hurry, so
everyone on the club bus, please.All aboard!

Well travel south from Delaware, then venture across the country westward, until we
reach California.
We can spend the next virtual month scouring the southwest for fossilized plant specimens,
while working
on our suntans.Next month, well
endeavor to cross the ocean to sunny Australia, then onto Asia and
other spots on the globe.

Whats
In a Name?

By general definition, petrified wood is tree material that has undergone mineralization.This could
loosely apply to man-made pressure-treated lumber or naturally preserved ancient kauri
wood from New
Zealand.More on that later.

Petrified wood is a fossil created by the replacement of a trees plant cell shapes
with minerals,
such as quartz, calcite, or pyrite.A stone
cast is left after the lignin and cellulose decay.Its
telltale
colorful grain patterns and concentric rings are fostered by staining minerals, such as
iron, manganese,
or copper.

Pure
silica exhibits a bluish-white hue.

The quartz variety predominates the worlds paleoforests.On the Mohs scale of hardness it rates
a 7, equal to quartz.It is tough, yet
brittle, breaking as does cryptocrystalline quartz.Amazingly,
it
can weigh many times that of a piece of similarly sized wood.[i]

Color
Chart:

Petrified
Wood comes in all colors of
the rainbow. The following minerals
give the wood it's characteristic palatte:

There are three main steps towards permineralization of living plant matter: (1.)
encapsulation,
or removal from an environment that causes decomposition, (2.) introduction of sufficient
quantity
of a mineral-laden solution to bring about chemical-biochemical replacement of cell
structure, and
(3.) time.

At what point during the petrification process (or preservation process) do we determine
that
wood is in fact petrified wood? Is
a partially or fully done process sufficient for our definition?Can
it be man-made, or is nature the sole producer?Or,
is age a factor?

There is a debate over whether certain, recently recovered wood from the ground has
actually
undergone the process of petrification.There
are three examples that come to mind.They
are:
New Zealand kauri wood, century-old sunken logs, and flood-covered landscape living tree
remnants.

The
first is the southern hemispheres millenias old kauri wood.Recently recovered or mined from the
peat bog-laden earth, ancient kauri (Agathis australis) is estimated by
radio-carbon dating to have been preserved in the ground for around 50,000
years.The only officially-licensed New
Zealand mining company explains that harvesting is state-monitored, so it is
rare and can be expensive.[iii]

Partial mineralization has occurred, thus giving this workable wood some superior degree
of hardness and a cognac-colored sheen that underscores a beginning to fossilization.Though not fully petrified, natural longer-scale
preservation has increased its beauty and value.Buried
under a peat swamp, after having lived for about 2,000 years, each tree has rested,
untouched since the last Ice Age.We
can compare the old wood to modern trees, as kauri still graces the New Zealand landscape.

One can both visit the living members at the Northland Forest Park,
and later procure online some ancient lumber from a hardwood vendor, Ancientwood,Ltd.
of La Pointe, Wisconsin, for use and study.If
you are keen on paleobotany, this job is for you.Some
folks enjoy working it as wood.

(Left): Agathis australis (Kauri tree)
from New Zealand, called 'Te Matua Ngahere' after the Maori 'Father of the Forest'
(wikipedia)

The
second is the spoils of latent logjams.For
about 100 years, some cut logs sent downriver
from antique logging transportation operations have sunk to river or lake bottoms, only to
have their
harvesting deferred to recent times.These
water-logged bonuses are fully useable in modern
carpentry and woodworking projects.Whether
some mineralization has occurred to harden the
lumber is at issue.

The
third is flood-preserved stands of trees.One
recent example are the remains of ancient forests that can be seen poking their highest
limbs above the lower water levels of Lake Powell in the awesome GlenCanyonNational
Recreation Area.These plants have
been submerged by man-made projects for about 40 years.
One could study these.

Naturally-occurring ancient examples are coastline forests, since sea-levels have risen
since times BCE. An inland example is the
shifting of water levels in Yosemite National Park.Dead stumps stand in testament to volcanic and
tectonic processes, perhaps preserved by dissolved volcanic gases or related
mineral-bearing waters.

As
an historic supervolcano in the west spewed an ash cloud into the believed prevailing
paleowinds, deposits reached as far east as Nebraska.I wonder if the process is occurring right
now under the fallen forest on the slopes of the currently active Mt. St. Helens
volcano at the Mt. St. Helens
National Monument in Washington state.

Pressure-treated
Lumber

Todays pressure-treated pine wood is just that, lumber infused with chemicals, like
chromated
copper arsenic (CCA), under intense pressure.These
minerals act to preserve the wood, thus making it resistant to insect infestation and
decay from ground and water contact.Some
lumber manufacturers guarantee their product for up to forty years!

Last year, during our clubs Junior Booth Labeling Party in preparation for our March 2005 Show,
I found a small piece of P-T pine.It was
used as a base to mount a mineral specimen, I believe. Determined to label it, I
suggested we sell it as petrified wood, as it was chemically-preserved wood.
Laughing, we put it back in the box, but didnt offer it for sale.

Here
is an example of a middleground two-fold process: man-made, then naturally lithified.A
story reported in Australias outback gives proof that planted timber fenceposts have
been partially
fossilized in recent history, thus giving credence to a faster than previously believed
permineralization
process occurring in nature.The 1918 flood
laid sediment and water conducive towards creating
fossilizing conditions.[iv]

Experimental
chemistry has brought petrification to the forefront of the news.A man-made
process has brought about a ceramic compound that mimics petrified wood. It is amazing
that
with a nearby petrified forest, that scientists in Washington state are creating
artificial petrified
wood.Why, do you ask?

Benefits
include filtering pollutants, acting as catalysts, and sponging up contamination.

The process involves hardening a softwood, such as pine or poplar,
bathing it in acid, then
soaking it in silica solution for days. After air-drying, it is cooked in an
argon-filled furnace to
1,400 degrees Celsius,

Many experimental and industrial crystals are grown in an argon
atmosphere. The replicated petwood consists of a new silicon carbide.[v]

In the article Instant Petrified Wood Yields Super Ceramics,

Materials scientists at the
Department of Energy's Pacific Northwest National
Laboratory have developed a chemical
process that adds a promising new dimension to the search for advanced catalyst
technologies,
as well as to cutting tools, abrasives and coatings.

These
laboratory versions of petrified wood borrow the best aspects of metal and carbon to
create a superstrong material that can take temperatures up to 1,400 degrees Celsius.They
create it in days, instead of millions of years.

The idea it to build ceramics on
wood templates.Silicon,
titanium, and argon are used.
The useable end products are silicon carbide (SiC) and titanium carbide (TiC).[vi]

The
amazing porosity of the material lends itself to use as a catalyst or a filter.This wood
flours can be infused with metals, creating better cutting tools.And, all this from a renewable
resource!What will they think of next?

So, a modified type of
truly petrified wood can be of use beyond its outward structure
and beauty.

Another application
touts a petrifying effect:

Both
a Popular
Science, October
1992 article, and U. S. Patent File #4,612,050,outline an
invention owned by Mr.
Hamilton Hicks of Greenwich, Connecticut, which explain
a process whereby
fresh wood can bealtered
by chemical solutions in the lab to create an analogous petrified wood.[vii]

His Sodium
silicate composition patent file abstract
reads: A mineralized sodium silicate
solution for the application to wood has a composition causing it to penetrate the wood
and jell
within the wood so as to give the wood the non-burning characteristics of petrified
wood.[viii]

Australian
scientists of Nanotec Pty. Ltd.
have devised a newly marketed product which they
tout repels water and UV rays.Their
Nanoseal Wood may be defined as man-made petrified,
but actually may serve as
building material.

It is a water
based, ultra hydrophobic, colloidal solution with self assembling properties to
form the functional surface structure.The repellent effect is
done by a combination of molecular
structural surface changes and added on hydrophobic properties.[ix]

The topically applied
liquid seals out air and moisture, thus halting decay, much like the
encapsulated environment in which petrified wood forms.One must ask how long will it last,
and are we creating petrified wood over time?

As
the vast Triassic paleoforest that spannedTexas
to Utah consisted of ancient conifers, somecomparison
can be logically made.Technology hasalmost
defeated the process of aerobic decay.Evendecades
old loblolly pine carpentered buildingmembers
encased in plaster harden with age.

The
afore-mentioned lab-created woods seem tomimic
natures processed pieces to a definingdegree of
form.So, are these cultured productsreally
comparable to this months favorite mineral?

Lets
review by reading a passage written about natural petrification, and see how it compares.

Sometimes
the original cellular structure is obliterated and what remains is simply a cast
of the original log; other times, growth rings, bark, knots, and even cellular structure
is
preserved with remarkable fidelity. This later, more detailed preservation is possible
because
silica and other inorganic molecules are much smaller than organic molecules; rather than
"molecule for molecule" replacement, the organic molecules are actually coated
and surrounded
with silica. Small amounts of impurities add color to the fossilized wood: yellow, brown
and red
indicate iron; black and purple take their hue from carbon or manganese.[x]

Doesnt
this describe
the major technical features of our chemists processes above?

In past articles, we have
mentioned substitutes for natures bounty, especially when
quantities are scarce.For example,
turquoise, diamond, and opal have all been man-made.
Though having uses beyond the gemstone, why should petrified wood be treated any
differently?

As stated above,
similar conditions around the globe create the environment to petrify wood.
It seems that all three main geologic processes contribute to the creation of our
preserved
paleoforests.Volcanic lava, ejecta, and
silicieous ash (igneous), soil and mud deposition
(sedimentary), and mineral-laden groundwater replacement casting (metamorphic), work in
sequence to bring about our painted landscapes of today.

Experts
differ as to the timeframe of formation.Some
believe that millions of years were
required; whereas, others cite instances of objects, such as modern fenceposts being
fossilized after floods.Most submit that
eons have passed before natural examples were
completely mineralized.

One of the most
studied areas is the Petrified Forest
National Park in Arizona.Stratigraphers
in one paper state that, two layers of the Upper Triassic Chinle Group containthe bulk of petwood
in the park.Also, the Sonsela Member of the
Petrified Forest Formationholds the more brightly
colored logs for which the park is known.

Though
scientists and theologians havedisagreed
over the age and specific event(s) thatproduced
the petrified forests of the world, manyseem to
agree on the composition of the finalproduct.Our goal is to focus upon the petrificationprocess
that occurred after the trees were buried,and upon
the colorful wonders that we see today.

The
references this author makes to prehistory are based both upon popular scientific
belief and upon the premise that perhaps some petrified wood formed before man.Even many
of the worlds cultural creation scenarios agree that plants existed before mankind;
therefore,
it could be possible that some petrified wood could have formed before, as well.

Lets
look at a couple of examples.One wood that
is
still known today, living in some of earths forests, isGingko.The Gingko Petrified Forest
State Park locatedon the
Columbia River in Washington State hostsMiocene
(5.3 to 23.8 mya) Ginkgos (Gingko biloba).[xii]

Another is
the Mississippi Petrified
Forest boasts Eocene Epoch (Tertiary) 36 million
year old wood.These primeval remnants of
perhaps a bald cypress forest (a tree known
today) lay testament to the passage of time.

Many
other species lie extinct, with evidence of their existence only culled from the
fossil record.This month, we will leave them
lie, in favor of space for more descriptive
pictures.I will introduce some of Linnean
scientific names, so that they will appear more
familiar to you in our next excursion.Next
month, well uncover more about paleobotany
and plant taxonomy.

In many
western states, falling volcanic ash covered living trees in thick sedimentary
layers.Over time, iron- and silica-laden
groundwater seeped into wood cells, thus causing
the mineral(s) to replace cell walls.This
gives us the brightly colored quartz logs we see
today.Perhaps the heat of lavaflows hastened
the process in some closer to the volcanic
cone.

In
the Petrified Forest
National Park, geologic uplifting of the Colorado plateau,
sedimentary erosion, and the surficial freeze-thaw cycle produces the fractured stone
logs,
as pictured here.[xiii]

Silicification
is the main process forming petrified wood, though others exist.For example,
coalification, calcification, and pyritization, happen, too.So, how do these other processes
compare to silicification?

Coalification
and bogs predominated the eastern climate, like in the massive coal areas
of Pennsylvania and Ohio, so fewer petwood areas were created for us to see now. Some
form seams, other more acidic conditions can produce coal balls.As erosion and uplifting
are key factors in releasing or exposing the layers in which lithified logs loom, our
eastern
paleoclimate

brought
less to the surface for us to dig.

The
exceptions are the present mountainous areas in the east, such as the Appalachian
Range.Its orogeny pushed rock
containing our favored fossil to collectable depths.(See the
list of states just
below)

When
logs are calcified, the resultant stones are white.Upon
exposure to the suns
UV rays over time,

United States law prohibits
collection of fossil, rock, and mineral materials from National
Parks and Monuments, unless specifically permitted. Each state, county, town, or
area has
their own rules pertaining to their public spaces, as well. Its always best to
study a guidebook,
a reliable websource, and inquire locally.

We
can access these online museums and sites on our laptops and PDAs in between
stops as we roll down the road:

We will
visit just a few of the various and sundry places.Youll
have to make side trips
on your own, as we have only four short weeks this month to explore, before we are ready
to
travel to other continents.(Yes, even to
Antarctica!)Well, here they are:

Arizona

Home to our featured locale, the Petrified Forest National
Park, Arizona, boasts some of the
more prevalently displayed petrified paleoforest landscapes on earth!Look below. Could these
two photographs taken by two different photographers at two different times be of the same
logs?

Much
of the area was set aside by President Theodore Roosevelt in 1906 as a National
Monument.In 1962, it became a National Park.[xvii]

Today, it is still tradition for any seated U. S. President to
declare a National Park to
conserve important lands and landmarks for the future. By
act of the State Legislature,
Araucarioxylon arizonicum is a fossil conifer that is
the state fossil
of Arizona.[xviii]

Together, these proclaimed symbols account for an historical place of grand note for all
of us to visit and enjoy.With an unspoiled
landscape, our roving eye might have us envision
a past, living environment.Tall trees
swaying, and earth-shaking creatures walking out of
past times, might spur us to move quickly, to avoid being trampled by these--dinosaurs!
At any time, we can open our minds eyes to the possibility,
or return to our current beauteous
desolation.With this exercise, we have
developed our paleo-view, to help us understand
more about our world.

Here, our paleo-viewpoint shows us that, In the Triassic
period, this species of tree
flourished in what is now known as the Black Forest, part of the 37,851 ha (93,492-acre) Petrified Forest
National Park in eastern Arizona. Prehistoric Arizona was a flat stretch of
tropical turf in the northwest corner of a supercontinent
known to modern geologists as Pangaea.[xix]

"Many
of the fossilized logs are from a tree called Araucarioxylon arizonicum. Two
others, Woodworthia and Schilderia, occur in small quantities in the
northern part of the
park. All three are now extinct.[xx]

The
park has seen man venture across its vastness over millennia, since the
end of the
dinos.From the Anasazi, Mogollon, and
Sinagua peoples up to 10,000 years ago, to the
sixteenth-century Spaniards,
up to modern times, many explorers and natives alike have
walked the park.[xxi]

Some Native American oral history recounts the role that petrified wood played in the
grand scheme.(We will visit these stories in
our next installment, so stay tuned.)

Now,
with a brief history and new perspective to our lovely land, lets feast our eyes on
its wonders!Look out the windows, this
is what you will see.Well disembark,
so everyone
take a bag lunch as you leave the bus.

Another
way to virtually tour the park is by obtaininga
copy ofthe 1936
Warner Brothers ganster movie The
PetrifiedForest,starring
Leslie Howard, Bette Davis, andHumphrey
Bogart.Itmight be
interesting to visit theshooting
locations in the parkafterwards,
to see if all thelogs
are all still in the same place!Ascollecting
is ano-no,
they should all still be.

Collecting rules in the park differ from outside its boundaries.

On other public or private land, generally permission is required tocollect.The wood may be collected over a large area
ofeast-central
Arizona, but outside of the National Park, most of thebest sites are privately owned. Petrified wood may be also found inUtah, in various locations around the Escalante River, and in theCoyote
Buttes region near the Paria River. Sometimes the wood ismuch
less colourful - for example, the specimens that occur in theBisti
Badlands in New Mexico - but just as interesting.[xxii]

Florida

As Florida has spent much of geologic history underwater, marine fossils are par for the
collecting course.However, petrified wood
may still be found in the state.And, the renownedThomas Farm Fossil
Preserve has uncovered various species of extinct vertebrates, as well.

For the kids, Dinosaur World
can be a relaxing respite from fossil hunting.With
activities
suchas a kid's
pretend fossil dig and a gift shop carrying petrified wood, you can take a breatherfrom
collecting, if youve a mind to.Me,
Im ready to go to the next state.Meet
me at the busin
an hour.

Texas & Louisiana

A European club, the Circle of Mineralogy and Paleontology of
Belgium (CMPB), has
reported on their Field Trip to Bryan,
Texas. They have even photographed a house there
built of plant fossils!

It is also good to know that, Petrified palmwood (Palmoxylon sp.),
is the state stone of Texas
and the official state
fossil of Louisiana.
It is from the Oligocene
epoch (34 - 23 mya)
and can be collected from many scattered sites in east Texas and western Louisiana.[xxiv]

North Dakota

John Bluemle writes in his web article North Dakotas Petrified
Wood, that petrified
wood is so common in North Dakota that is a nuisance to farmers, yet lines many a
driveway.
Mr. Bluemle also offers some locales to see our favorite fossil:

Utah

Utahs Brushy Basin
and Yellow Cat Flats
lay claim to the very rare Yellow Cat Redwood.
These Grand County Jurassic-Triassic rocks hold some beautiful reddish specimens.
Northeast of Moab, near the Henry Mountains, the Morrison
formation holds shales,
mudstones and sandstones that play host to fossil plant treasures that have eroded from
their volcanic ash matrix.[xxvi]

Washington

Volcanism plies the modern Washington landscape, as it had in the geologic past.
Various lava flows have preserved layer upon layer of sunken, waterlogged trunks of
cypress, oak, elm, and gingko that grew in the paleoswamps. Water and silica from
these events, combined like chocolate and peanut butter, to make a new composite material:
petrified wood. Now the state gem, we can visit it at the Gingko
Petrified Forest State Park in Vantage.[xxvii]

Much like us
today, on our Grand Excursion into the Petrified Forests, famous explorers
of the past have traversed these painted grounds to discover our quarry:
Petrified Wood!

Did Lewis & Clark
venture through any petrified forests?Yes,
according the John Bluemles
article, Lewis & Clark,
Geology, and North Dakota, Lewis wrote in his April 16, 1805 journal
entry that he had found a partially coalified and petrified wood around the Sanish area.[xxviii]

In 1853, U. S. Army Lieutenant Amiel Weeks Whipple led
a survey expedition into the
southwest to chart land suitable for completion of a coast-to-coast railroad. An
excursion
with the self-same practical goal of improving mass-transit (Find the Northwest
Passage!),
while exploring the country, Whipple lead a team, including a geologist, to map a
prospective
route. He trekked across what would be known later as the Petrified Forest National Park.

Whipple's party crossed the path of
today's Interstate 40 somewhere around Pinta and
entered what is now the Petrified Forest National Park north of the highway. They
more or
less paralleled the highway for 15-20 miles and crossed back to the south side of the
highway
path near where it crosses Lithodendron Wash. Camp 76 was probably west of
Pinta in what
is today called Dead Wash before they the Park.

Here's
some of what Whipple had to say:

December
2--Camp 76...Quite a forest of
petrified trees was discovered to-day, prostrate
and partly buried in deposits of red marl. They are converted into beautiful
specimens of
variegated jasper. One trunk was measured ten feet in diameter, and more than one
hundred
feet in length. Some of the stumps appear as if they had been charred by fire
before being
converted to stone. The main portions of the trees have dark brown color; the smaller
branches
are of a reddish hue. Fragments are strewn over the surface for miles.[xxix]

Were
there other famous wild west personalities and artistic observers?No doubt.Youll
just have to follow our links and ask folks along the way about their stories.I know I love stories.

Including us, I was fortunate enough to contact several people, who were happy to help
with the success of this expeditious article.They
have shared with us pictures, paintings,
and sculpture.As youve heard the
adage, A pictures speaks a thousand words, you can
see the experience of petrified wood through their eyes.

One such group is the
Provencherfamily.Chris, Candida, and
their childrenkeep a websitewith
photos of their
family adventures.Like many American
families, theychoose to visit or
vacation at parks andnatural
landmarks.Their trip to thePetrified Forest
National Park hasproducedsome wonderful
images thatthey have
chosen to share with us here.

One artist, Scott W. Parker,
travels tofamous U.
S. locations to find his muse.He hasalso captured images
of the PFNPin 2003 in
his photography, paintings, anddrawings.Heembarks on
various travelprojects for his
studies.His currentproject is
a three-month survey of the Gulfof Mexico,
finishing up in April 2006.

Parker
hopes to bring his National Parks Collection not only to galleries across the United
States, but also to schools, where he believes his work can educate and most
inspire.

I
cant forget the Kenfields, who,
sincethe
1950's have brought lapidary work withpetrified
wood to a new height.Theirmusic boxes
just rock (forgive the pun).

With a
lifelong pursuit of what they callthe rock
hobby, the Kenfield brothers assembled a collection of
petrified wood
and fossils from around the world.They havemastered
the handcrafting of musicboxes,
made entirely of petrified wood! The Kenfields also paint and create petwood
framed art. They
offer you a gallery and museumexperience.And, they support rockhoundeducation
with their Junior
Rockhound Club.

You
can visit their collection at ThePetrified
Wood Gallery,
Ogalalla,Nebraska.

Photographer,
Christy Marx,
hashelped us to get a
close-up view of thiswondrous
stone. Her adventures into the
Petrifed Forest have delivered some very
spectacular images!

She
makes its beautytransportable
via her photograph prints.As we are
wont to carry outhuge logs enmasse from
collecting locales outside of the park, to perhaps improve our own home or even our
gardens
landscape, we realize we mightonly procure smaller
specimens, unless we have a crane.Whata delight, though, to
have one of her large
prints gracing our indoor
retreat!

Steve
Speer and his family atSticks-in-Stones
Lapidary atSticks-in-Stones.com
havegenerouslyallowed us
to show items from theirtravels in petwood.Their stand-updisplaysbring out the grain
facing to giveus the
feel of wood.

Dr.
Stephen Ervin, Professor ofZoology 
Emeritus at CSU, has a goal topromoteeducation and
evolution,especially
with petrified woods fromaround the world
as ateaching tool.Hehas agreed
to share any and all picturesof his fine fossil
collection,from which
wemight learn about
plants and more.

Last,
but not least, our fellow clubmember and fossil
dealer, GeneHartstein,
hastraveled in his
gathering ofmaterial
to offer us at our upcomingMarch 4-5, 2006 Show.Gene was kindenough to dig up some
extra photos,especially
of our clubs normalcollectingarea, of
Delaware petrified wood.

(Left): Gene Hartstein stands on a local petrifed log that
he collected on one of our club's fieldtrips Odessa, Delaware

We have
covered some man-made analogs that offer technologic breakthroughs that,
when applied, can help us to preserve our current environment from industrial
pollutants.
Since we leave natures product on the ground, we conserve on two levels!

A broader use
of petrified wood is as a symbol. To promote state identity, at least six
states have officially made either their state fossil, mineral, stone, or gemstone.
They are:
Arizona, Louisiana, Mississippi, North Dakota, Texas, and Washington.[xxx]

As we have seen, petrified wood comes in a variety of
mineralizations, each with their own
best methods to work. Most material available is quartz-like, and could be lapped
accordingly.

Agate, jasper,
quartz, chalcedony, and opal
are all mineral forms of silicon dioxide with color
impurities.

These characteristics give petwood its beauty, of course, only after nature's cast.

Some of the
carbonate and pyrite rough may or may not be suitable for lapidary work. But
if you decide to give it a try, please be careful, as pyritized wood might spark and wear
down
your sharp tools. Possibly, it could work like the metal that it is.

Until Next Time

We hope you have enjoyed traipsing
the countryside and scouring museums in our search
for all the forms of petrified wood. Perhaps you'll take one of the many side-trips,
or work up
some logs in the lap lab. Don't be late for next month's trip. We shall board
a jet and travel to
world locales for exotic petrified wood. See you then!
Until then, stay safe, and happy collecting.

Article Contributors:

I would like to gratefully acknowledge the generous
contributions of our fellow Strontianite
enthusiasts,
collectors, authors, curators, professionals, and club members who made this
work possible. Thanks.

About the Author:

Ken is current webmaster of the Delaware
Mineralogical Society.He has a diploma in
Jewelry Repair, Fabrication & Stonesetting from the Bowman Technical School,
Lancaster, PA, and worked as jeweler.He has
also studied geology at the University of Delaware.And,
he is currently a member of the Delaware Mineralogical Society and the Franklin-Ogdensburg
Mineralogical Society. E-mail: kencasey98@yahoo.com.

Want to see your name in print? Want to co-author, contribute,
or author a whole Mineral of the Month
article? Well, this the forum for you!

And Members, if you have pictures, or a story you would like to
share, please feel free to offer. We'd like to post them for our mutual enjoyment.
Of course, you get full photo and author credit, and a chance to reach other
collectors, hobbyists, and scientists. We only ask that you check your facts, give
credit where it is due, keep it wholesome for our Junior Members watching, and keep on
topic regarding rockhounding.

You don't even have to be experienced in making a webpage. We
can work together to publish your story. A handwritten short story with a Polaroid
will do. If you do fancier, a text document with a digital photo will suit, as well.
Sharing is the groundwork from which we can get your story out there.

Our club's webpages can reach any person surfing the net in the
world, and even on the International Space Station, if they have a mind to view our
website!

We are hoping for a possible tie-in to other informative programs
upon which our fellow members might want to collaborate. Contact any officer or
board member with your suggestions.

Our next MOTM will
be "Petrified Wood: Part II".
For 2006, we are waiting for your suggestions. What mineral do you want to know more about?

____________________________________

Most of the Mineral of the Month
selections have come from most recent club fieldtrips and March Show Themes, and from
inspiring world locales and people, thus far. If you have a suggestion for a future Mineral of the Month, please e-mail me
at: kencasey98@yahoo.com, or tell me at our next meeting.